Determining Active and Passive Pressures
Transcript of Determining Active and Passive Pressures
Determining Active and Passive Pressures for Cohesion and
Cohesionless Soils Using Variation for a Smooth Wall
by Farid A. Chouery,1 P.E., S.E.
©2012 by Farid A. Chouery all rights reserved
Abstract
Variational method is used to determine active and passive forces for a smooth wall with
a cohesionless and cohesive back fill. The resulting slip surface shows that the extremum
of the force occurs when the slip surface is the Coulomb line for a level backfill. The
analysis shows that to achieve the Coulomb line the internal shear in the slices must be
zero. For a sloped backfill with cohesion the resulting slip surface is not a line. Adding
internal shear in the slices for the passive condition with a sloped backfill with a
cohesiveless material is examined and compared with log-spiral method. For special
boundary conditions, where the slip surface cannot be a line, the forces, the slip surface,
the pressure on the wall and the location of the resultant on the wall are obtained for
active and passive conditions. The method is adequate and will always give the derived
forces and slip surfaces.
Introduction
The problem of active and passive earth pressure for a smooth wall has been solved by
Coulomb theory (1776) [4], Rankine theory (1857) [8], and log-spiral theory after
Terzaghi (1941 & 1943) [11,12]. These theories are presented in most soil mechanics’
1 Structural, Electrical and Foundation Engineer, FAC Systems Inc., 6738 19th Ave. NW, Seattle, WA
2
texts [12,13]. Each of these methods involves assuming a line slip surface as an
approximation of a more complex surface as observed in both model tests and field
observations. The reason in the differences between these slip surface methods and the
laboratory is in the laboratory the observed slip surface is that of a slope stability problem
and not of a wall pressure problem. In this paper, a more general solution to the problem
is developed using variational methods using slices. In variational method, a general form
of failure surface is derived, and then "varied" until the extreme condition of pressure on
a wall is found. In a similar approach, variational method has been used to find the factor
of safety in slope stability: Baker and Garber (1978) [1] and numerical methods by
Leshechinsky (1990) [6]. The pressure discussed in this paper is for homogenous soil for
a smooth wall. It can be readily extended to multilayer soil. However, further work is
required. The limitation of the variational method is that it assumes a continuous function
for the slip surface. This can be a problem for a heterogynous material as seen in Fig. 1.
The method fails and
FIG. 1 - Heterogynous Material with Slip Surfaces
Slip Surfaces
3
revisions are needed, possibly piecewise functions are needed. Note: piesewise continous
function will be needed for multilayer homogenous soil. The general methodology has
been classically to find the extremum for the earth pressure by finding a slip surface
where a potentially soil failure would occur for extremum pressure. Thus, the design has
captured the worst condition for the force on the wall. Historically, this method has been
used satisfactorily provided the material properties have been reached. It is impossible in
practice to test for all the soil friction values and cohesion through borings logs, thus
engineering judgment has to be made for these values. In order to use the method
proposed properly and interpret the results, care has to be taken in selecting the material
properties.
With the variational method, [15], one selects arbitrary admissible slip surfaces and
determines the forces acting on the boundary of the earth mass. The definitive slip surface
is one that yields an extremum value for the earth pressure. In this paper, variational
methods are used to determine the slip surface, based on some practical assumptions. The
solution shows that the Coulomb wedge is a particular case of the general solution
presented here. It is believed that the application of variational methods to earth pressure
problems is a practical advancement to understanding of retaining wall problems. Five
different analyses will be done to avoid giving one cumbersome general equation and
give a closed form solution for the special cases. In analysis 1 a closed form solution is
reached, it is assumed a level backfill for cohesive and cohesiveless material, which is
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useful for most site conditions. Analysis 2 is for a sloped backfill and slanted wall for
cohesiveless material, which does not include cohesion to give a closed form solution.
Analysis 3 is repeating analysis 2 with cohesion where the pressure is not given in a
closed form but can be obtained numerically. In analysis 4 a closed form solution is
reached for passive earth pressure condition for sloped backfill with cohesiveless material
to include internal vertical shear from the slope backfill. Analysis 5 is a repeat of Analysis
4 with cohesion.
Analysis 1
In this analysis, it is desired not to restrict the slip surface to a line and to find a function
y(x) that would extremize E, as shown in Fig. 2(a). It is assumed that the wall moves
dE
dW
y(x)
dx0
(0,y )
x
y
dx
T
EE
TdW
0
n
n
n+1
n+1
α
α
α
α−φ
φ
Proposed Slip Surface A Slice
FIG. 2(a) FIG. 2(b)
dQ
( )x y0 1,
FIG. 2 – Slip Surface for Level Backfill
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sufficiently such that the friction between the wedges equal 0. Thus, Tn+1 = Tn , as in Fig.
2(b), for all the wedges. Since the wall has no friction, Ti = 0 for all the wedges. This
assumption is similar to the assumptions used in stability analysis by the method of slices
(Bishop (1955) [2]) and in analysis of passive earth pressures for a wall with friction by
Shields and Tolunay (1973) [10]. If the Ti 's are to be included in the derivations, K0 can
be determined using incipient shear method. Thus, each slice is in equilibrium, so the
overturning moment remains in balance and not of concern.
Thus, the force dE can be written as
[ ])tan(sincos)tan(1 φαααφα −+−−==−+ cdsdWdEEE nn ................................ (1)
Replacing dW by γydx and ds by dx/cosα and integrating yields
[ ]{ }∫ −+−−=0
0)tan(tan1)tan(
x
dxcyE φααγφα ...................................................... (2)
or
( )dxcyE
x
∫
+
−+−
+−
=0
0 tantan1
tantantan1
tantan1
tantan
φαφαα
γφαφα
................ ...................... (3)
Now tanα = − = ′dy
dxy ................................................................................................ (4)
Substituting Eq. 4 in Eq. 3 yields
( )dx
y
yycy
y
yE
x
∫
′−−′−′
−−′−−′−
=0
0 tan1
tan1
tan1
tan
φφ
γφφ
.................................................... (5)
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Eq. 5 can written as:
( )dx
yycy
yE
x
∫
′−
+′−−−
′−+
−=0
0 22 tan1sin
1 cot
sin
11
tan1
cottancot
φφφ
φγ
φφφ
φ
…………………………………… (6)
It is necessary to find the extremum of E in Eq. 6 for the boundary condition:
(i) Given (0, y0) and (x0, y1), find the slip surface that passes through these points.
(ii) Given (0, y0) and P0 located somewhere on a given line x = x0 or a line y = y1,
find the slip surface.
Therefore Euler’s equation [15] applies where
( )
0 and
tan1sin
1 cot
sin
11
tan1
cottancot
22
=
′
ℜ−
ℜ
′−
+′−−−
′−+
−=ℜ
ydx
d
y
yycy
y
∂∂
∂∂
φφφ
φγ
φφφ
φ
.............. (7)
which can be written as ℜ − ′ℜ
′=y
yh
∂∂ 0 ............................................................... (8)
where ℜ does not involve x explicitly, and h0 is a constant.
Substituting in Eq. 8 yields
7
( )
( ) ( ) 0222
2
22
tan1sin
tan
tan1sin
1cot
tan1costan1
cottancot
hy
y
yc
yy
y
y
=
′−
′−
′−+−−
′−
′+
′−+
−
φφφ
φφφ
γφφφ
φφφ
....................... (9)
Eq. 9 reduces to the following:
( )( ) ( )2
02 tan1tan1tan2 φφγφ yhcyyy ′−=+−′+′ ...................................................... (10)
or
( )( ) ( )2
0 tan1)tan(cos/1tancos/1tan φφγφφφφ yhcyyy ′−=+−+′++′ ................... (11)
Note Eq. 10 is a parabola in ′y . From Eq. 11: h y0 0 1≥ ′ ≤ − − for tan / cosφ φ or
′ ≥ − +y tan / cosφ φ1 , and h y0 0 1 1< − − ≤ ′ ≤ − + for tan / cos tan / cosφ φ φ φ . From
trigonometric identity
( )( )tan tan
/ cos /
sin /
sin
costan
cos
π φ π φ π φπ φ
φφ
φφ4 2
2
2
1 2
2
1 1±
=
±
=
− ±
±=
±= ± + ......... (12)
From Eq. 11 and Eq. 12, ( )h0 0 4 2 4 2≥ ≥ + ≤ − − for or α π φ α π φ/ / / / , and
( )h0 0 4 2 4 2< − − ≤ ≤ + for π φ α π φ/ / / / . Taking α to be positive yields the
following bound on h0 :
2/4/0for 0 and , 2/4/for 0 00 φπαφπα +≤≤<+≥≥ hh ......Active............. (13)
8
For the passive condition, replacing φ by −φ and c by –c in Eq. 11 yields
2/4/0for 0 and , 2/4/for 0 00 φπαφπα −≤≤<−≥≥ hh ......Passive............ (14)
The slip surface can be derived by rewriting Eq. 10 to
( ) ( ) ( ) 0tan2tan 1122
1 =+−′++′− hyyhyyhy φφ ....................................................... (15)
where φγ
φγtan
and
tan1
01
hh
y
c
hh =
+= is a new constant. Rewriting Eq. 15 in
′ ′x y instead of yields (See Appendix I)
hc
y
cy
x
++
+±=′
φγ
φγφ
φ
tan
tan
cos
1tan …………………………………………………. (16)
If h = 0 in Eq. 16, then ′x becomes a constant and y(x) must follow the Coulomb wedge.
Since ′ = −x cotα and α π φ= +/ /4 2 for a Coulomb wedge it follows from Eq. 12 that
( ) ( )′ = − + = − − = −x cot / / tan / / tan / cosπ φ π φ φ φ4 2 4 2 1 ................................. (17)
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In order to satisfy Eq. 17, the plus sign in Eq. 16 can be dropped, and the equations
become
hc
y
cy
x
++
+−=′
φγ
φγφ
φ
tan
tan
cos
1tan ..............Active........................................... (18a)
For the passive condition, replacing φ by −φ and c by –c
hc
y
cy
x
++
+−−=′
φγ
φγφ
φ
tan
tan
cos
1tan ..............Passive.......................................... (18b)
Integrating Eq. 18a yields the slip surface equation
khc
yc
yhc
yh
cyh
cyyx
+
+
++
++
+−
++
+−=
φγφγφγ
φγφγφφ
tan2
tantan2ln
2
tantancos
1tan
2
2
...................................... (19)
where k is the constant of integration. Substituting the point at x = 0 y = y0 yields
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khc
yc
yhc
yh
cyh
cyyk
+
+
++
++
+−
++
++−=
φγφγφγ
φγφγφφ
tan2
tantan2ln
2
tantancos
1tan
00
2
0
0
2
00
................................ (20)
and the active slip surface, Eq. 19, becomes
+
++
++
+
+
++
++
+
−
++
+−
++
+−−=
hc
yc
yhc
y
hc
yc
yhc
yh
cyh
cy
cyh
cyyyx
φγφγφγ
φγφγφγ
φγφγφγφγφφ
tan2
tantan2
tan2
tantan2
ln2
tantantantancos
1tan)(
00
2
0
2
0
2
0
2
0
…………………….. (21a)
For passive it becomes
+
++
++
+
+
++
++
+
−
++
+−
++
+−−−=
hc
yc
yhc
y
hc
yc
yhc
yh
cyh
cy
cyh
cyyyx
φγφγφγ
φγφγφγ
φγφγφγφγφφ
tan2
tantan2
tan2
tantan2
ln2
tantantantancos
1tan)(
00
2
0
2
0
2
0
2
0
……………...………………..(21b)
To find the active force E, Eq. 5 can be rewritten in terms of ′ ′x y instead of ,
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dy dx instead of , and the interval [ ] instead of [ ] , where y x y0 0 10 0, , is taken to be 0 in
Fig. 2(a). Thus
( )dy
x
xcyx
x
xE
y∫
′−
′++′
′−
′+=
02
0 tan
1
tan
tan1
φγ
φφ
.......................................................................................... (22)
Substituting Eq. 18a in Eq. 22 and rearranging yields
dy
cyh
cy
hc
y
c
dy
cyh
cy
hc
y
yE
y
y
∫
∫
++
+
+
+
−−
++
+
+
+
−+=
0
0
0 2
0 22
2
tantan
tan2
cos
1tan2
tantan
tan2
cos
tan
cos
1tan
φγφγ
φγφ
φ
φγφγ
φγφφ
φφγ
......................................................... (23)
Thus the mathematical pressure q ydE
dy( ) = , from each slice to another, becomes
++
+
+
+
−−
++
+
+
+
−+==
φγφγ
φγφ
φ
φγφγ
φγφφ
φφγ
tantan
tan2
cos
1tan2
tantan
tan2
cos
tan
cos
1tan)(
2
22
2
cyh
cy
hc
y
c
cyh
cy
hc
y
ydy
dEyq
12
..................................................... (24)
It is desired to investigate the extremum of q(y) with respect to h, thus
0 yields 0 == hdh
dq ..................................................................................................... (25)
Thus the extremum occurs at the Coulomb wedge for passive and active. Hence it has
been shown that the Coulomb wedge is the wedge for a smooth wall that moves
sufficiently such that Tn+1 = Tn . It is noted that all of Ti = 0 since the wall is smooth. For
other prescribed conditions (i) and (ii) above it is necessary to use the slip surface of Eqs.
21a-b. Integrating Eq. 23 yields the active force
φγφγφγ
φγφγφγ
φφ
γ
φγφγφγφγφγφγφφ
γ
φφ
φγ
tan
2
tantan2
tan2
tantan2
ln4cos
tan
tantan2tantantan2tancos
tan
tan2cos
1tan
2
2
00
2
02
2
0
2
00
02
220
ch
ch
c
cyh
cyh
cy
h
ch
chccyh
cy
hcy
cyy
E
++
+
+++
++
+
−
+
−−
++
+
−+−
+
+=
……………………….…............. (26a)
and the passive force
13
φγφγφγ
φγφγφγ
φφ
γ
φγφγφγφγφγφγφφ
γ
φφ
φγ
tan
2
tantan2
tan2
tantan2
ln4cos
tan
tantan2tantantan2tancos
tan
tan2cos
1tan
2
2
00
2
02
2
0
2
00
02
220
ch
ch
c
cyh
cyh
cy
h
ch
chccyh
cy
hcy
cyy
E
++
+
+++
++
+
+
+
−−
++
+
−++
+
+=
……………………………............ (26b)
Note: that the right hand term involving h in Eqs. 26a-b has a minimum at h=0. It is
desired to show that for φγ tan
ch −< the slip surface does not reach the top of ground at
the point (x0,0). It has been shown in Eqs. 13 and 14 that if h0 < 0 (or h < 0), then
α π φ α π φ≤ + ≤ −/ / / /4 2 4 2 for active, and for passive. Thus a slip surface with
φγ tan
ch −< is further than the triangle Coulomb wedge as shown in Fig. 3.
x0
y1
CoulombWedge
45+φ/2
Slip Surface for h < 0
Slip Surface
FIG 3 – Slip Surface for Level Backfill with Constraint h < 0
14
Furthermore, Eq. 18a-b shows that ′ = ∞ ′ =x y or 0 at some value φγ tan
chy −−= .
Since φγ tan
ch −< , the y value must be positive and cannot be 0. Thus y is below
ground. Also, for φγ tan
chy −−< the term h
cy ++
φγ tan is not defined in Eq. 18a-b.
Thus for φγ tan
ch −< Eqs. 26a-b are not applicable.
Eq. 22 must be integrated from y0 to y1 instead of y0 to 0, where the point (x0, y1) is a
point underground. This integration yields
+++
++
+
+++
++
+
−
++
+
−+−
++
+
−+−
−+
+
−=
φγφγφγ
φγφγφγ
φφ
γ
φγφγφγ
φγφγφγφφ
γ
φφ
φγ
tan2
tantan2
tan2
tantan2
ln4cos
tan
tantan2tan
tantan2tancos
tan
tan)(2cos
1tan
22
11
2
1
00
2
02
1
2
11
0
2
00
102
221
20
cyh
cyh
cy
cyh
cyh
cy
h
cyh
cy
hcy
cyh
cy
hcy
yycyy
E
..................................Active.................................... (27a)
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+++
++
+
+++
++
+
+
++
+
−+−
++
+
−++
−+
+
−=
φγφγφγ
φγφγφγ
φφ
γ
φγφγφγ
φγφγφγφφ
γ
φφ
φγ
tan2
tantan2
tan2
tantan2
ln4cos
tan
tantan2tan
tantan2tancos
tan
tan)(2cos
1tan
22
11
2
1
00
2
02
1
2
11
0
2
00
102
221
20
cyh
cyh
cy
cyh
cyh
cy
h
cyh
cy
hcy
cyh
cy
hcy
yycyy
E
..................................Passive.................................. (27b)
Thus it can be easily concluded that h = 0 is the only minimum of the h terms in Eqs.
26a-b. Hence E has a maximum at h = 0 for active and a minimum at h = 0 for passive.
This shows that the Coulomb wedge gives the extremum for E as it has been shown in
Eq. 25.
Condition (i)
It is seen that Eqs. 18a-b , 21a-b , 26a-b , and 27a-b are useful for condition (i) when the
slip surface must pass through a point and physically is not represented by the Coulomb
wedge. The following examples have this situation:
Example 1 Consider Fig. 4, where the passive pressure is to be calculated for a slip
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x0
y0
y2
45−φ/2
(0,y0)
(x0,0)
Slip Surface of Eq. 31-b
Basement Wall
FIG. 4 – Slip Surface for Passive with and Existing Basement Constrained Example 1
surface that is controlled by the presence of a basement wall. The Coulomb wedge cannot
physically go through the wall. Thus the general slip surface is applicable.
In this situation y0, x0 are known. Thus, substituting their values in Eq. 21b yields
x y y hyh h
y hy y h0 0 0
20
02
0 0
1
2 2 2= + + +
+ + +
tan
coslnφ
φ ................................ (28)
The value h can be obtained numerically from Eq. 28, and E can be calculated from Eq.
26b. Thus, if γ = 120 pcf (1.93 g/cm3), φ = 30 degrees, c = 0, y0 = 10 ft (3.05 m), and x0 =
10 ft (3.05 m), then from Eq. 28, h = 27.3318 ft (8.3307 m). Taking λ = h y/ 0 = 2.73321
in Eq. 26b gives E = 21,455 plf (31.97 g/m). If a straight line is used from (0, y0) to (x0,
0), then α = 45 degrees. Evaluating the Coulomb wedge y = y0 = 10 ft (3.05 m) gives E =
22,392 plf (33.37 g/m). Note that Eq. 26b gives the extremum with 4.4% difference over
the straight line. Note: If treated as the full wedge with Kp = 3 where y = 5.77ft (1.76 m)
is triangular pressure and 4.33 ft (1.29 m) is pressure with surcharge then E = 18,000 pfl
(26.82 g/m). In this situation it is assumed the wall is rigid thus the slip surface is a curve
and E = 21,455 plf (31.97 g/m).
17
Example 2 Consider Fig. 5, where a slip surface passing through (0, y0) to (x0, y1) must
y0=20
x0=5
y1=5
line 2line 1
71.565 deg
(x0,y1)
(0,y0)
FIG. 5 – Slip Surface for Active with and Existing Basement Constrained Example 2
be analyzed for an active condition. γ = 120 pcf (1.93 g/cm3), and φ = 30 degrees, c = 0.
From Eq. 21a substituting y0 = 20 ft (6.1 m), x = x0 = 5 ft (1.52 m), y = y1 = 5 ft (1.52 m),
and calculating numerically h = 6.88284 ft (2.0979 m). Substituting in Eq. 27a gives E =
6,740 plf (10.05 g/m). If comparing with a straight line, line 1, from (0, y0) to (x0, y1), it
gives E = 6,651 plf (9.91 g/m), where the Coulomb wedge was used with W =
.5(5+20)(5)(120)=7,500 plf (11.18 g/m), and α = 71.565 degrees. Thus, a 1.3% difference
over the derived is obtained. To find Emax further analysis must be done for line 2 and the
result must be compared with line 1.
Example 3 In the case of stability analysis for tieback wall, as shown in Fig. 6(a) , the
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ψ
ξ
ψ
α
Q
WT
Pa
y0
x0
y2
paW
y1
Pa
pa
T
Q
E
W
Anchor
Soldier Pile
Tieback WallFIG. 6-a
Force DiagramFIG. 6-b
ξ
FIG. 6 - Slip Surface to Determine Safety Factor of a one Tieback Wall
slip surface is shown to pass through the point in the middle of the anchor, see reference
[3,7,9,16]. In this case the stability factor Tmax/Tdesign is to be calculated as in reference
[16]. From the force diagram, Fig. 6(b), the summation of horizontal and vertical forces
are
p T Q Pa a+ + =cos sinξ ψ ........................................................................................ (29)
T Q Wsin cosξ ψ+ = ................................................................................................ (30)
Substituting Q from Eq. 30 in Eq. 29 yields
19
TP W pa a=
− −
−
tan
cos sin tan
ψξ ξ ψ
............................................................................................... (31)
From Eq. 31 T = Tmax can be calculated where W Etanψ = of Eq. 27a, and the constant h
can be found from Eq. 21a for a given (x0, y1). W can be calculated numerically from
integrating the right hand side of Eq. 21a from y1 to y0
W y x f y dyy
y
= + ∫γ γ1 01
0
( ) ........................................................................................... (32)
where f(y) is the right hand side of Eq. 21a. Thus, ψ =
−tan 1 E
W,
p ya = −
1
2 4 212 2γ
π φtan , and P ya = −
1
2 4 202 2γ
π φtan .
Taking for example y0 = 20 ft (6.1 m), γ = 120 pcf (1.93 g/cm3), φ = 30 degrees, c = 0, ξ =
20 degrees, Tdesign = 3,872 plf (5.77 g/m), Pa = .333(120)(20)(20)/2 = 8,000 plf (11.92
g/m), y2 = 6 ft (1.83 m), x0 = 15 ft (4.57 m), y1 = 6 + 15 tan(20) = 11.46 ft (3.49 m), pa =
.333(120)(11.46)(11.46)/2 = 2,626 plf (3.91 g/m), and substituting x = x0 = 15 ft (4.57
m), and y = y1 = 11.46 ft (3.49 m) in Eq. 21a gives h = -10.8507 ft (-3.3073 m).
Substituting in Eq. 27a gives E = 154.4 plf (0.23 g/m). Integrating Eq. 32 numerically
gives W = 26,802 plf (39.94 g/m). Thus, ψ = 0.3301 degrees, and T in Eq. 31 becomes
5,566 plf (8.3 g/m). The stability factor Tmax/Tdesign = 5,566/3,872 = 1.438. If using a
straight line method, where ψ in Eq. 31 becomes α−φ, α = 29.66 degrees, and W =
0.5γ(y0+y1)x0 = 28,314 plf (42.2 g/m), then T = 5,885 plf (8.77 g/m), and the stability
20
factor = 5,885/3,872 = 1.52. This gives 6% difference in the safety factor over the derived
method.
Condition (ii)
For condition (ii), where the slip surface must pass through a line at x0 or at y1 below x0 ,
it yields ∂∂ℜ
′=
=y
x x0
0, or from Eq. 7
( ) ( )
( )0
coscot
tan1
tan
0cottan1sin
tan
tan1cos
2
2
1
2222
1
=−′−
+
=+′−
−′−
−
γφφ
φφγ
φφφ
φφφ
γ
c
y
cy
or
cy
cy
y
....................................... (33)
Substituting Eq. 18a with y1 instead of y in Eq. 33 where ′ = ′x y1 / yields
0tantancos
1
tantan
2
11 =−
+−++
φγφγφφγφ
ccyh
cy ……….....active….... (34a)
0tantancos
1
tantan
2
11 =−
+−++−
φγφγφφγφ
ccyh
cy ……...passive……. (34b)
Thus
21
+
±
+=
φγφγφφ
φγφφ
tantancos
tan2
tantan2tan
2
221
ch
cchy
.............................................................................................. (35)
At ∞→y& 0→x& then
φγφ
tantan 2
2
chy −= ...................only active ........................................................ (35a)
Substitute Eq. 35 in Eq. 21a and 21b for a given x0 and find h. If y1 is negative then y1 = 0
and h can be calculated from Eq. 21a and 21b for a given x0. If y1 is above y2 then y2
controls and find h from Eq. 21a and 21b. Note: y1 is zero only if h = 0 and c = 0. Thus, it
can be obtained from Eq. 34a is the following problem: Consider that the slip surface
must pass through a line at x = x0 and have y h12= tan φ below x0 and c = 0. This makes
′ = ′ = ∞x y0 or in Eq. 18a. This condition can occur in the real world as seen in
example 4 below, and E can be obtained from Eq. 27a. Note y h12= tan φ with c = 0 is
invalid for passive pressure, since Eq. 44b is not zero. For passive Eq. 45 is not valid
when replacing φ by −φ and c by –c and the slip surface must pass through the point (x0,
0) when there is a rigid obstacle otherwise it can be analysed as a surcharge problem as
seen in example 1.
For φγ tan
1
chy −−= , h < 0 and ′ = ′ = ∞y x0 or in Eq. 18a-b. This situation can happen
if the slip surface must pass through a line x = x0 where the slope must be zero at y1 below
x0 . Fig. 7 shows such an example of an passive condition with c = 0, where the concrete
22
x0
y0
y1 Concrete Mat
y' =0
FIG. 7 – Slip Surface for Passive with Mat Slab Constrained Special Condition
mat shown on top can sustain itself. Thus at the line x = x0 , ′ =y 0 due to deformation. In
this example the weight of the slab is taken to be the same as the weight of soil.
Substituting c = 0, h = -y1 and y = y1 in Eq. 21b yields
( )
−+−−−+−−=
1001
2
0
1101
2
0010
22ln
2cos
1tan
yyyyy
yyyyyyyx
φφ ............ (36)
and the passive force E can be obtained from Eq. 27b:
−+−+−
++
1
1001
2
02
101
2
01
0
22ln
42cos
tan
y
yyyyyyyyy
yy
φφγ
............................................................................................................. (37)
Example 4 Consider Fig. 8, where the active pressure is to be calculated for a slip surface
+
−=
φφγ
2
22
1
2
0
cos
1tan
22
yyE
23
x0
y0
y1
y3
(0,y0)
(x0,y1)
Basement Wall45+φ/2
FIG. 8 – Slip Surface for Active with a Neighboring Structure Example 4
that avoids the basement wall with c = 0. This problem is also similar to finding the
active pressure for a wall adjacent to rocks.
From Eq. 35
h y= 12cot φ .............................................................................................................. (38)
Substituting Eq. 38 in Eq. 21a yields
24
( )( )x
yz
zz
z z
z z
0
0
22 2
2 21
11
2
2 2
2 1 2= − − − + −
+ +
+ + +
tan
cos sincot
cotln
/ sin cot
cot cotφ
φ φφ
φ φ φ
φ φ
..................................................................................................... (39)
where z = y1/y0 . Thus, for a given x0 and y0 , z can be calculated numerically from Eq. 39.
Taking h y zy= =12
02cot cotφ φ , it can be substituted in Eq. 27a to give the active force.
Taking for example y0 = 20 ft (6.1 m), γ = 120 pcf (1.92 g/cm3), φ = 30 degrees, c = 0, x0
= 5 ft (1.52 m), gives z = 0.12475, y1 = 2.495 ft (76.05 cm), and h = 7.484 ft (228.14
cm). Substituting in Eq. 27a gives E = 6,777 plf (10.1 g/m). If a line is taken from (0, y0)
to (x0, 0), using the Coulomb wedge, it gives E = 6,530 plf (9.73 g/m), a 3.8% difference
over the derived. Now if a Coulomb method is used with y3 as shown in Fig. 8, the wedge
can be taken as the Coulomb line with a uniform surcharge γy3 . This gives E = 5,428 plf
(8.09 g/m), where the overburden y3 = 11.34 ft (3.46 m). Thus, the Coulomb wedge does
not give Emax and a difference of 25% is obtained over the derived.
For condition (ii), where the slip surface must pass through a line y = y1, ℜ in Eq. 7 can
be rewritten as
′−
′+−′−′
′−
′+−=ℜ
x
xxcxy
x
x
φφ
φφ
γtan
tan1
tan
tan1 .................................................................. (40)
If the Euler Eq. is used with Eq. 40, the same slip surface will be obtained. Thus, for a
slip surface passing through a line y = y1, it yields
25
∂∂ℜ
′=
=xy y1
0 ................................................................................................................. (41)
Executing Eq. 41 on Eq. 40 yields
( ) ( )0
)(tan
1tan2
)(tan
1tan2tan2
2
2
2
1 =′−
−′−′−
′−
−′−′
x
xxc
x
xxy
φφ
φφφ
γ .............................................. (42)
Thus,
′ = ± + = ±=x y y1
2 11
tan tan tancos
φ φφ
.................................................................. (43)
This forces h in Eq. 16 to be zero, or the Coulomb wedge is the solution for this
condition. This situation is similar to having a uniform surcharge at the line y = y1. This
confirms that the Coulomb wedge is the proper slip surface as described in Eq. 25 and in
the extremum of Eq. 26.
Analysis 2
For a sloped smooth wall with a sloped back fill with c = 0 (see Fig. 9(a)) the slip surface
26
x tan(β−θ) β−θ
β
α
φ
α−φ
α−φ
(0,y0)
(x0,y1)
dE
dWcosdWsin
TTi+1
i
θθ
θ θ
θdWcos
dE
dWsindQ
dQ
Proposed Slip SurfaceFIG. 9(a)
Force DiagramFIG. 9(b)
x
y
FIG. 9 - Slip Surface with a Sloped Backfill and Slanted Wall
for an active condition can be derived similarly. It is assumed that Ti = Ti+1 with T0 = 0.
From the force diagram, Fig. 9(b), it yields
( )[ ]dE dW= − +cos tan sinθ α φ θ ............................................................................. (44)
Thus,
( )[ ] ( )[ ]E y x dxx
= − + + −∫γ θ α φ θ β θcos tan sin tan0
0
............................................. (45)
where ( )[ ]dW y x dx= + −tan β θ . Eq. 45 can be rewritten as
27
E ku
uudx
x
= −′ +− ′
∫γ θ
ζφ
θ4 0 10
sintan
tancos .................................................................... (46)
where ( )k4 1= + −tan tanφ β θ , ζ φ β θ= − + , ( )[ ]u y x k= + −tan /β θ 4 , and
[ ]′ = ′ + −u y ktan( ) /β θ 4 . From variational method, and repeating the same analysis as in
analysis 1, it yields
dx
duk
u
u h= −
+tanφ 1 ............................................................................................... (47)
and the slip surface
khuhuuh
huukux +
+++−+−= 22ln2
tan 221φ ........................................ (48)
where ( )[ ] ( )k1 1= + −tan tan tan / tan tanφ ζ φ ζ θ , and k is the constant of integration.
Substituting Eq. 47 in Eq. 46 and rewriting yields
E k k ku h
u huudu
u
u
= −+
+
∫γ 4 3 2 2
2
1
0
.............................................................................. (49)
where
u y k0 0 4= / ,
( )[ ]u y x k1 1 0 4= + −tan /β θ ,
28
( )( )k2 1= + −cos tan tan tan tan tanθ φ ζ φ ζ θ , and
( )k3 1 2= − + +sin tan cos tan tanθ φ θ ζ φ .
Note E is maximum at h = 0, giving the slip surface to be the Coulomb wedge. Thus the
application of β and θ is the same as in Coulomb. Validation of the solution at h = 0 can
be checked numerically against US Army Corps Publication EM 1110-2-2502 Equation
3-13 and 3-19 as a different mathematical form of the same solution. Terzaghi (1943)
[12], Rosenfarb and Chen ( 1972) [9] show for high β and θ = 0 on a smooth wall, the
slip surface is not a line and produces lower Kp values. However, for Ka values the
differences were negligible. This means that the Ti's due to the ramp are not zero in
passive condition. This is possible for a high β > 0 influencing the slice contact shear at
the ramp. Equations derived for these conditions are shown in analyses 4 and 5 below.
Evaluating E in Eq. 49 yields
E k ku u
k k uh
u hu= −
− −
+
γ γ4 3
02
12
4 2 0 02
02 2 2
− −
+ +
+ + +
+ + +
uh
u huh u hu u h
u hu u h1 1
21
20
20 0
12
1 12 4
2 2
2 2ln
........................................................................................................ (50)
For passive replace φ by φ− and E becomes:
29
+
−+
−= 0
2
0024
2
1
2
034
222huu
hukk
uukkE γγ
+++
+++++
−−huhuu
huhuuhhuu
hu
11
2
1
00
2
02
1
2
11
22
22ln
42
........................................................................................................ (51)
For condition (i) described before, the constant h and k can be obtained by substituting
the two end points (0, u0) and (x0, u1) in the Eq. 48. For condition (ii): It is of merit to
obtain the general solution, for the undetermined points, for a given curve and not just for
a line. Some practical applications would be a buried vault, tunnel, tank, utility, etc. , that
would interfere with the coulomb line. Suppose the given curve is g0(x, y) = 0. By
substituting for y k u x= − −4 tan( )β θ in g0(x, y), the new function will be g(x, u) = 0. If
the end point (x0, u1) is obtained, then y1 can be obtained from y k u x1 4 1 0= − −tan( )β θ .
From reference [15] the following condition must be satisfied for condition (ii):
[ ]∂∂
∂∂
∂∂
∂∂
ℜ
′−
ℜ
+ ′=
=
==
= =
u
g
u
g
xu
g
ux x
u u
x x
x x u u
0
1
0
0 1
1
0 ................................................................................ (52)
where ℜ is the integrand of Eq. 46. Doing the mathematics of Eq. 52, and solving for ′u1
and using a relation for h from Eq. 47, yields
30
hR u k
R u kR u
u u=−
− + −+
−
−1
11
1 12
1 11
2
1 1
( ) cot
( )( )( tan tan )
(tan tan )
φ
φ θζ θ
.................................................. (53)
where
R u
g x u
x
g x u
u
x x
u u
( )
( , )
( , )10
1
==
=
∂∂
∂∂
................................................................................................. (54)
R(u1) is a function of u1 alone is because x0 can be determined from g(x0, u1) = 0. Now, k
in Eq. 48 is determined from the point (0, u0). Thus, substituting Eq. 52 in Eq. 48 and
replacing (x, y) by (x0, u1) gives an equation with u1 as the only unknown. Hence, u1 can
be determined (numerically).
The following are two important functions:
A line: [ ]y ax b k u a x b g x u= + → − − + − = = change to
4 0tan( ) ( , )β θ
from Eq 63
→ = −− +
R ua
k( )
tan( )1
4
β θ .......................................... (55)
A circle: ( ) ( ) ( ) ( tan( ) )x x y y r x x k u x y rc c c c− + − = → − + − − − − =2 2 2 24
2 2 0 to β θ
31
[ ]
to → =
−
− − −−
−R u
x x
k k u x y k
c
c
( )tan( )
tan( )1
0
4 4 1 0 4β θ
β θ ................ (56)
where x0 can be determined from the quadratic equation in g(x0, u1) = 0.
The following equations are the results for the condition where k4 = 0:
Eq. 45 yields:
Ek
uudx
x
= + +′
∫γ θ θ φsin cos cot 5
0
0
......................................................................... (57)
dx
du
h
u
k
k= − 6
52 ............................................................................................................ (58)
kuk
kuhx +−=
5
6
2ln ................................................................................................ (59)
E kh
u
k
ku du
u
u
= −
∫γ 5
26
2
540
1
......................................................................................... (60)
( )Ek
ku u k h
u
u= − −γ γ6
2
50
21
25
2 0
18ln ............................................................................ (61)
where ( )u y x= + −tan β θ , ′ = ′ + −u y tan( )β θ , u y0 0= , ( )u y x1 1 0= + −tan β θ ,
k52= cos / sinθ φ , ( )k6 = −cos / sinθ φ φ , and k is the constant of integration. For passive
replace φ by φ− . For Condition (ii):
hk R u
k
u
R u= − − −
1 1
26 1
5
2
1
1
( )
( ) ............................................................................... (62)
32
where R(u1) is of Eq. 54. To obtain the solution for a line or a circle, set k4 = 1 in Eqs. 55
and 56, and u1 can be determined numerically from Eq. 58.
For the passive condition replace φ by −φ in the above equations, starting with Eq. 44.
It is noteworthy that if the axis in Fig. 9(a) is rotated by −(β−θ), the new axis will be
( ) ( )x y x= − − + −sin cosβ θ β θ , ( ) ( )y y x= − + −cos sinβ θ β θ , and
( ) ( )x x y= − + −cos sinβ θ β θ . If substituting for the new axis in the slip surface of Eq.
48, the resulting slip surface is similar to what has been obtained in Eq. 19, only with
different constant values.
Analysis 3
When repeating analysis 2 with cohesion the Eq. 44 become:
[ ] [ ]dscdWdE )tan(sincossin)tan(cos φαααθφαθ −+−+−= ………………… (63)
Or
( )∫
−+
−−+−
+
−+
−=0
1 tan1
tan)tan(1sincos
tan1
tan44
u
udx
u
uukcu
u
ukE
&
&&
&
&
φζ
θβθθφζ
γ
………………………………….. (64)
And the variational equation becomes:
33
0)(2)( 63522
41 =+++−+ auauauauaua && …………………………..…………… (65)
Where:
( )( )
( )( )
( )hca
hca
hca
ka
ka
ka
−−=
−−−−=
−−−−−
−=
−=
+=
6
5
24
43
42
241
tan)tan(tantantan
)tan(tantantantantan
tantancos
tantantancos
tantantancos
φθβφζφθβφθφζφ
ζθθγ
ζθφθγ
φφθθγ
…………………………….. (66)
Thus the maximum E occurs at
63
41
2
63
52
63
52
aua
aua
aua
aua
aua
aua
du
dx
++
−
+
+−
+
+= ……………………………………….. (67)
This clearly Eq. 67 will not produce a line slip surface for c not equal zero and h = 0 also
it can be shown that h cannot be zero for maximum or minimum E. Validation of the
solution at h = 0 can be checked numerically against US Army Corps Publication EM
1110-2-2502 Equation 3-25 as a different mathematical form of the same solution.
34
Analysis 4
For a sloped smooth wall with a sloped back fill with c = 0 (as in Fig. 9(a)) the slip
surface for a passive condition can be derived similarly for shear due to the ramp. It is
assumed that
xdxKx
Kdx
dTi tan
cos
)(tantancos
cos
)tan(
2
1 2
0
2
0 φθ
θβφθ
θθβ −
=
−= ………….… (68)
Where the shear is assumed to occur from an average at rest pressure
)sin1(06.10 φ−=K on the ramp subtracting from the weight dW. From the force yields
( )[ ]θφαθ sintancos ++= dWdE ............................................................................. (69)
Thus,
( )[ ][ ]∫ +++=0
0sintancos
x
dxAxyE θφαθγ ............................................................. (70)
where ( ) dxxKydxAxydW
−−−+=+= φ
θθβ
θβ tancos
)(tantan)(
2
0 . Where
( ) φθ
θβθβ tan
cos
)(tantan
2
0
−−−= KA . Eq. 70 can be rewritten as
udxu
ukE
x
∫
′+
+′−=
0
04 costan1
tansin θ
φζ
θγ .................................................................... (71)
35
where φtan14 Ak −= ,
−−−−−= − φ
θθβ
θβφζ tancos
)(tan)tan(tan
2
01 K ,
[ ] 4/ kAxyu += , and [ ] 4/ kAyu +′=′ . From variational method, and repeating the same
analysis as in analysis 1, it yields
hu
uk
du
dx
+−−= 1tanφ ............................................................................................... (72)
and the slip surface
khuhuuh
huukux +
+++−+−−= 22ln2
tan 221φ ........................................ (73)
where ( )[ ] ( )ζθφζφ tantan/tantantan11 −−=k , and k is the constant of integration.
Substituting Eq. 72 in Eq. 71 and rewriting yields
∫
+
++=
0
1 2234
2u
uudu
huu
hukkkE γ .............................................................................. (74)
where
u y k0 0 4= / ,
[ ] 4011 / kAxyu += ,
( )( )ζθφζφθ tantantantan1tancos2 −−=k , and
( )φζθφθ tantan21costansin3 −+=k .
36
For E Eq. 51 applies.
Note: E is minimum at h = 0, giving the slip surface to be a line. Note: as the slip surface
approach the top surface the shear of Eq. 68 at y < 0 can be reduced. If h = 0 is used in
Eq. 51 it yields:
2
0
4
2
2
0
4
3
2y
k
ky
k
kE γγ += ………………………………………………………. (75)
In here 4
00
k
yu = and 01 =u , comparing with log-spiral in Table 1 at 0>= βφ and
0=θ yields:
Table 1 shows a maximum %5± difference between log-spiral and Eq. 75.
TABLE 1 – Passive Pressure Coefficient Kp for Sloped Backfill 0>= βφ and 0=θ
φ (degrees) Kp (Coluomb) Kp (log-spiral) Kp (Eq. 75)
10 1.704 1.642 1.697
15 2.321 2.170 2.284
20 3.312 3.119 3.172
25 5.074 4.822 4.600
30 8.743 7.472 7.107
35 18.82 12.67 12.14
40 70.92 23.58 24.84
37
Analysis 5
Analysis 5 can be done similar to analysis 4. Where the ramp shear is
−+
−= xc
xK
dx
dTi )tan(tancos
cos
)tan(
2
12
0 θβφθθθβ
…………………… (76)
Or
dxcxdxKTi )tan( tancos
)(tan 2
0 θβφθ
θβ−−
−−= …………. Passive ………… (77)
Surcharge
If there is a uniform surcharge q on top of the wall, it can be replaced by soil such that the
soil thickness above y is y qs = / γ . Thus y becomes y ys+ in the integral equations. By
making a change of variable y y yt s= + , the results will be similar and the equations
easily modifiable.
Wall Pressure
The location of the Coulomb force is at (2/3)y0 from the top of wall for triangular
pressure. This is a reasonable assumption since Ka is independent of y0, yielding dE/dy0 =
γKay0. However, this method is not applicable for examples 1, 2 and 3. A different
approach is necessary in order to find the pressure. This can be done by moving down the
wall from the top at incremental distances y + ∆y, and find the potential slip surfaces, and
forces. Thus, a table of Ej and yj can be created. The stresses at a distance yj can be taken
as (Ej − Ej-1) / (yj − yj-1). This will give the same result as in a Coulomb condition. For
38
example 1, 2, and 3, this method will take into account the Coulomb conditions at the top
of the wall. One needs to examine the wall boundaries and movements before using the
method. The following considerations need to be examined: (1) The potential slip
surfaces above y0 assumes the friction is almost fully mobilized. (2) The friction on the
wall may vary. It may not be constant throughout. (3) No abrupt changes in deflection
(the wall is continuous). In assumption (1), the friction on the bottom of the slice is φ φ'≤ .
However, if the wall movements indicate the entire wedge is either active or passive, then
φ' ≅ φ. φ' ≠ φ because the soil above and below yj are moving together resulting in the
apparent slip surface on the bottom of the wall. However, they must be close. In
consideration (2), even on a Coulomb wedge, if the friction of the wall varies it will
produce non-linear pressure.
Irregular Backfill
If the wall does not have a level or sloped backfill but an irregular backfill, the analysis
will require a computer program algorithm. One possibility is to use Fourier Series
converted to a Taylor Series on the top surface and proceed to solve the Euler equation.
Conclusion
Variational method has been used to determine active and passive forces for a smooth
wall with a cohesive and cohesionless soil. The methods are classical, conventional, and
only practical assumptions were used. The resulting slip surface shows that the extremum
of the force for a level backfill occurs when the slip surface is the Coulomb line for
cohesion and cohesionless soil. Additionally, in order to have the Coulomb failure
39
surface, the internal shear in the Bishop slices is required to be zero. For a sloped backfill
the resulting slip surface shows that the extremum of the force occurs when the slip
surface is a curve for cohesion soil and also when the internal shear in the Bishop slices is
not zero. When adding the internal shear due to a sloped backfill for a cohesiveless
material on a vertical wall the passive pressure is in good agreement with log spiral
method; however, the slip surface is still a line.
For special cases where the slip surface is dictated by physical conditions and must pass
through a point, a line or a curve, the forces and the slip surface can be obtained for both
active and passive conditions. Also, a method of calculating the pressures on the wall is
given. It can be seen that this method is adequate and will always give the derived slip
surface. It has been noted in the examples given that the derived slip surface has not
produced a significant difference over using a straight line. Although these differences are
of desirable accuracies, having the correct slip surface is important when considering the
influence of neighboring structures, activities, or discontinuities. If the engineer decides
to use a conservative pressure by ignoring the neighboring structure and use a slip surface
such that the neighboring structures do not exist, then the analysis given in this paper
should guide the engineer on the differences in the pressures and give him the necessary
comfort factor.
40
Appendix I
0tan
tan21
212 =
+
−−′−′
hy
hyxx
φφ
Solving the quadratic equation yields
1
212 tan
tantanhy
hyx
+
−+±=′
φφφ
or
1cos
1tan
hy
yx
+±=′
φφ
or
hc
y
cy
x
++
+±=′
φγ
φγφ
φ
tan
tan
cos
1tan
41
Appendix II.-References
1. Baker, R. and Garber, M. (1978). "Theoretical Analysis of the Stability of Slopes,"
Géotechnique, 28, No. 4, London, England, pp. 395-411.
2. Bishop, A. W. (1955). "The Use of Slip Circle in the Stability Analysis Analysis of
Slopes," Géotechnique, London, England, Vol. 5, No. 1, pp. 7-18.
3. Broms, B. B. (1968). "Swedish Tie-Back System for Sheet Pile Walls," Proc. 3rd
Budapest Conf. Soil Mech. Found. Eng., Budapest, pp. 391-403.
4. Coulomb, Charles Augustin (1776). "Essai sur une application des règles de maximis
et minimis à quelques problèmes de statique relatifs à l'architecture," Mem. Div.
Savants, Acad. Sci., Paris, Vol. 7.
5. Kranz, E. (1953). "Über die Verankerung von Spundwänden," 2 Auflage, Mitteilungen
aus dem Gebiete des Wasserbaues und der Baugrundforschung, Heft 11, Berlin: With,
Ernst and Sohn.
6. Leshchinsky, D. (1990). "Slope Stability Analysis: Generalized Approch," Journal of
Geotechnical Engineering, ASCE, Vol. 116, No. 5, pp. 851-867.
7. Ranke, A., and Ostermayer, H. (1968)." Beitrag zur Stabilitäts-Untersuchung mehrfach
verankerter Baugrubenumschliessungen" (A Contribution to the Stability Calculation
on Multiple Tie-Back Walls), Die Bautechnick, Vol. 45, No. 10, pp. 341-349.
8. Rankine, W. J. M. (1857). "On the stability of loose earth," Trans. Royal Soc., London,
147.
9. Rosenfarb, J. L., and W. F. Chen (1972). "Limit Analysis Solutions of Earth Pressure
Problems," Fritz Laboratory Roport No. 355.14, Lehigh University, pp. 53.
42
10. Shields, D. H., and Tolunay A. Z. (1973). "Passive Pressure Coefficients by Method of
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Appendix III.- Notation
The following symbols are used in this paper:
α = angle of the failure wedge, or of failure a slice, with the horizontal;
A = constant;
A = slope of line equation ( y = ax + b );
β = angle from the horizontal for ramp of soil on top of wall;
B = the y-axis intercept of line equation ( y = ax + b );
C = cohesion;
∆y = incremental vertical distance;
E = horizontal active force on the wall to maintain equilibrium;
Ei = horizontal active force on a slice to maintain equilibrium;
Ej = horizontal active force on wall at distance yj;
φ = angle of internal friction of soil;
φ' = immobile angle of friction soil;
f(y) = mathematical function in calculating the weight of soil in the slip surface;
γ = soil unit weight;
C = cohesion
g(x, u) = curve function where the slip surface must pass through in (x, u) coordinates;
g0(x, y) = curve function where the slip surface must pass through in (x, y) coordinates;
H = mathematical coefficient in the slip surface equations related to h0;
h0 = mathematical coefficient in the slip surface equations;
44
I = integer counter;
J = integer counter;
K0 = at rest earth pressure coefficient;
K = constant of integration;
k1 to k6 = mathematical coefficient for representations slip surface and active force Eq.'s;
Ka = active earth pressure coefficient;
Kp = passive earth pressure coefficient;
λ = dimensionless coefficient;
N = integer counter;
Pa = horizontal active force on a tieback wall to maintain equilibrium;
pa = horizontal active force above center of tieback grout length;
Q = reactive force on bottom of failure wedge or slice to maintain equilibrium;
Q = uniform surcharge pressure on top of wall;
q(y) = mathematical horizontal pressure function;
ℜ = calculus of variation function of mixed variables representing the integrand;
R(u1) = a non dimensional function = ( / ) / ( / )∂ ∂ ∂ ∂g x g u u u x x at and = =1 0 ;
R = the radius of a circle;
θ = angle from the vertical for slant wall;
T = Tmax;
Tdesign = design tieback tension force;
Ti = vertical shearing force on a slice to maintain equilibrium;
Tmax = maximum tieback tension force to failure;
45
U = new variable of distance as function of x and y;
u0 = y0;
u1 = new variable of distance as function of x0 and y1;
W = vertical force from soil weight;
ξ = tieback angle from horizontal;
X = coordinate x-axis;
x = rotated coordinate of x-axis;
x0 = x-coordinate at the end of the slip surface on top of the wall or in the soil;
xc = the x-coordinate of the center of a circle;
ψ = directional angle from the vertical for the reactive force Q;
Y = coordinate y-axis;
y = rotated coordinate of y-axis;
y0 = height of wall;
y1 = y-coordinate point on the end of the slip surface in the soil;
y2 = distance from top of the wall to tieback at face of the wall;
y3 = distance from top of the wall to Coulomb wedge;
yc = the y-coordinate of the center of a circle;
yj = the y + ∆y incremental distance on the wall for active force Ej;
ys = equivalent soil height to produce surcharge pressure q;
yt = y + ys;
ζ = φ − β + θ; and
Z = dimensionless coefficient.